Aulacopleura

Last updated

Aulacopleura
Aulacopleura konincki.jpg
Aulacopleura koninckii, Kosov u Berouna, Czech Republic
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Class: Trilobita
Order: Proetida
Family: Aulacopleuridae
Genus: Aulacopleura
Hawle & Corda, 1847
Type species
Arethusa koninckii
Barrande, 1846
Species
  • A. koninckii(Barrande, 1846)
  • A. andersoniAdrian & Chatterton, 1995
  • A. kriziŠnajdr, 1975
  • A. letmathensisBasse & Lemke, 1996
  • A. pogsoniEdgecombe & Sherwin, 2001
  • A. sandfordiEdgecombe & Sherwin, 2001
  • A. wulongensisWang, 1989
Synonyms

ArethusaBarrande, 1846 non De Montfort, 1808, ArethusinaBarrande, 1852

Contents

Aulacopleura is a genus of proetid trilobite [1] that lived from the Middle Ordovician to the Middle Devonian. Some authors may classify this group as subgenus Otarion (Aulacopleura). [2] The cephalon is semicircular or semielliptical, with border and preglabellar field. The glabella is short, with or without defined eye ridges connecting it with eyes of variable size. Spines at the rear outer corners of the cephalon (or genal spines) are present, typically reaching back to the 2nd to 4th thorax segment. The 'palate' (or hypostome) is not connected to the dorsal shield of the cephalon (or natant). The cephalon is pitted, or has small tubercles. The thorax has up to 22 segments. The pleural ends are usually rounded. The pygidium is small (micropygous), with an even margin. A. koninckii had a modern type of compound eye. [3]

Taxonomy

Barrande described Arethusa koninckii in 1846. However, Arethusa was occupied since it was used by De Montfort in 1808 for a foram protist. Barrande tried to correct this by proposing Arethusina as a replacement, but by that time that Hawle and Corda had already suggested Aulacopleura in 1847, which is thus the senior available name. [4] [5]

Distribution

See also

Related Research Articles

<span class="mw-page-title-main">Trilobite</span> Class of extinct, Paleozoic arthropods

Trilobites are extinct marine arthropods that form the class Trilobita. Trilobites form one of the earliest known groups of arthropods. The first appearance of trilobites in the fossil record defines the base of the Atdabanian stage of the Early Cambrian period and they flourished throughout the lower Paleozoic before slipping into a long decline, when, during the Devonian, all trilobite orders except the Proetida died out. The last extant trilobites finally disappeared in the mass extinction at the end of the Permian about 251.9 million years ago. Trilobites were among the most successful of all early animals, existing in oceans for almost 270 million years, with over 22,000 species having been described.

<span class="mw-page-title-main">Phacopidae</span> Extinct family of trilobites

Phacopidae is a family of phacopid trilobites that ranges from the Lower Ordovician to the Upper Devonian, with representatives in all paleocontinents.

<i>Phacops</i> Genus of arthropods (fossil)

Phacops is a genus of trilobites in the order Phacopida, family Phacopidae, that lived in Europe, northwestern Africa, North and South America and China from the Late Ordovician until the very end of the Devonian, with a broader time range described from the Late Ordovician. It was a rounded animal, with a globose head and large eyes, and probably fed on detritus. Phacops is often found rolled up ("volvation"), a biological defense mechanism that is widespread among smaller trilobites but further perfected in this genus.

<i>Naraoia</i> Extinct genus of arthropods

Naraoia is a genus of small to average size marine arthropods within the family Naraoiidae, that lived from the early Cambrian to the late Silurian period. The species are characterized by a large alimentary system and sideways oriented antennas.

Eoagnostus is an extinct genus from a well-known class of fossil marine arthropods, the trilobites. It lived during the terminal Lower Cambrian (Toyonian), until the earliest Middle Cambrian.

<i>Yunnanocephalus</i> Extinct genus of trilobites

Yunnanocephalus is a genus of ptychopariid trilobite. It lived during the late Atdabanian and Botomian stages, in what are currently Antarctica, Australia and China. It was a "moderately common" member of the Chengjiang Fauna. Yunnanocephalus is the only genus currently assigned to the Yunnanocephalidae family.

<span class="mw-page-title-main">Holochroal eye</span>

Holochroal eyes are compound eyes with many tiny lenses. They are the oldest and most common type of trilobite eye, and found in all orders of trilobite from the Cambrian to the Permian periods. Lenses covered a curved, kidney-shaped visual surface in a hexagonal close packing system, with a single corneal membrane covering all lenses. Unlike in schizochroal eyes, adjacent lenses were in direct contact with one another. Lens shape generally depended on cuticle thickness. The lenses of trilobites with thin cuticles were thin and biconvex, whereas those with thick cuticles had thick lenses, which in extreme cases, could be thick columns with the outer surface flattened and the inner surface hemispherical. Regardless of lens thickness, however, the point at which light was focused was roughly the same distance below the lens.

Plumulites is an extinct genus of machaeridians, extinct annelid group.

<i>Bumastus</i> Extinct genus of trilobites

Bumastus is an extinct genus of corynexochid trilobites which existed from the Early Ordovician period to the Late Silurian period. They were relatively large trilobites, reaching a length of 6 in (15 cm). They were distinctive for their highly globular, smooth-surfaced exoskeleton. They possessed well-developed, large compound eyes and were believed to have dwelled in shallow-water sediments in life.

<i>Conocoryphe</i>

Conocoryphe is a genus of primarily eyeless trilobites belonging to the family Conocoryphidae. They lived during the Middle Cambrian period, about 505 million years ago. These arthropods lived on the sea bottom (epifaunal) and lived off dead particulate organic matter.

<i>Bojoscutellum</i> Genus of trilobites

Bojoscutellum is a genus of trilobites in the order Corynexochida family Styginidae.

<i>Odontochile</i> Genus of trilobites

Odontochile is a genus of trilobites in the order Phacopida, family Dalmanitidae.

<i>Lejopyge laevigata</i> Extinct species of trilobite

Lejopyge laevigata is a species of agnostid trilobite belonging to the genus Lejopyge. It existed during the Guzhangian to the Paibian Age of the Cambrian. It has a cosmopolitan distribution and is an important index fossil in biostratigraphy.

<span class="mw-page-title-main">Eodiscina</span>

Eodiscina is trilobite suborder. The Eodiscina first developed near the end of the Lower Cambrian period and became extinct at the end of the Middle Cambrian. Species are tiny to small, and have a thorax of two or three segments. Eodiscina includes six families classified under one superfamily, Eodiscoidea.

<i>Pleuroctenium</i>

Pleuroctenium Hawle & Corda (1847) is an agnostid trilobite belonging to the family Condylopygidae Raymond (1913). The genus occurs in Middle Cambrian (Drumian) strata of Canada, the Czech Republic, England and Wales, France, and Sweden.

Diplorrhina Hawle and Corda (1847) is a genus of trilobite belonging to Order Agnostida. It lived during the early Middle Cambrian in what are now the Czech Republic and the North Siberian plateau. as in members of the family Peronopsidae it lacks a preglabellar furrow. Both cephalon and pygidium lack spines. It is difficult to distinguish Diplorrhina from many other peronopsids.

<span class="mw-page-title-main">Cyclopygidae</span> Extinct family of trilobites

Cyclopygidae is a family of asaphid trilobites from the Ordovician. Cyclopygids had an extratropical distribution, and there is evidence that they lived in darker parts of the water column. Cyclopygids are characterized by enlarged eyes, with a wide angle of view, both horizontal and vertical, reminiscent of the eyes of dragonflies. These typically touch the glabella directly on the side. Cyclopygids all lack genal spines, but Symphysops carries a forward directed frontal spine on the glabella. It is presumed that at least the members of the genus Pricyclopyge swam upside down and had bioluminescent organs on the third thorax segment. Cyclopygids had between 7 and 5 thorax segments, a wide and stout axis, and short side lobes.

<i>Viaphacops</i>

Viaphacops is a genus of trilobites in the order Phacopida, family Phacopidae, that lived during the Middle Devonian, and is known from North and South America, Asia.

<i>Entomaspis</i> Extinct genus of trilobites

Entomaspis is an extinct genus of harpetid trilobite from Upper Cambrian to Early Ordovician marine strata of the United States. Species are typified by their proportionally large, vaulted, croissant-shaped or bonnet-shaped cephalons that have the cheeks freed to become elongated, curved librigenial spines, and by their comparatively large, crescent-shaped eyes.

2021 in arthropod paleontology is a list of new arthropod fossil taxa, including arachnids, crustaceans, insects, trilobites, and other arthropods that were announced or described, as well as other significant arthropod paleontological discoveries and events which occurred in 2021.

References

  1. Sam M. Gon III. "Trilobite info". www.trilobites.info.
  2. Fossilworks: Aulacopleura Hawle and Corda 1847 (trilobite)
  3. Schoenemann, Brigitte; Clarkson, Euan N. K. (2020-08-13). "Insights into a 429-million-year-old compound eye". Scientific Reports. Springer Science and Business Media LLC. 10 (1). doi:10.1038/s41598-020-69219-0. ISSN   2045-2322. PMC   7426942 .
  4. Moore, Raymond C., ed. (1959). Treatise on Invertebrate Paleontology [ Part O - Arthropoda 1 (Arthropoda General Features, Protarthropoda, Euarthropoda General Features, Trilobitomorpha)]. Geological Society of America and University of Kansas Press.
  5. B. W. Hayward: Arethusa Montfort, 1808 †, on: World Foraminifera Database, marinespecies.org, Flanders Marine Institute
  6. 1 2 Edgecombe, G.D.; Sherwin, L. (2001). "Early Silurian (Llandovery) trilobites from the Cotton Formation, near Forbes, New South Wales, Australia". Alcheringa: An Australasian Journal of Palaeontology. 25 (1): 87–105). doi:10.1080/03115510108619215. S2CID   128404133.
  7. 1 2 3 Hong, Paul S.; Hughes, Nigel C.; Sheets, H. David (2014). "Size, shape, and systematics of the Silurian trilobite Aulacopleura koninckii". Journal of Paleontology. Cambridge University Press (CUP). 88 (6): 1120–1138. doi:10.1666/13-142. ISSN   0022-3360.
  8. Schoenemann, Brigitte; Clarkson, Euan N. K. (2020-08-13). "Insights into a 429-million-year-old compound eye". Scientific Reports. Springer Science and Business Media LLC. 10 (1). doi:10.1038/s41598-020-69219-0. ISSN   2045-2322. PMC   7426942 .
  9. Marshall, Michael (2020-08-13). "Trilobites living 429 million years ago had eyes like modern insects". New Scientist.
  10. Fusco, Giuseppe; Hong, Paul S.; Hughes, Nigel C. (2016-05-06). "Axial growth gradients across the postprotaspid ontogeny of the Silurian trilobite Aulacopleura koninckii". Paleobiology. Cambridge University Press (CUP). 42 (3): 426–438. doi:10.1017/pab.2016.5. ISSN   0094-8373.
  11. Anderson, Natali (2020-08-17). "Silurian Trilobite Had Modern Type of Compound Eye - Paleontology". Sci.News.
  12. Šnajdr, Milan. New Trilobita from the Llandovery at Hýskov in the Beroun area, Central Bohemia (Czech). In: Vestník Ústredního Ústavu geologického 50(5). Praha, 1975. PP. 311-316. Pascal Francis (cnrs)
  13. BioLib: Aulacopleura krizi Šnajdr, 1975

Sources